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任意空间取向TI介质中速度随方位变化特征
引用本文:郝重涛,姚陈,王迅.任意空间取向TI介质中速度随方位变化特征[J].地球物理学进展,2006,21(2):524-530.
作者姓名:郝重涛  姚陈  王迅
作者单位:( 中国地震局地质研究所,北京 100029)
基金项目:国家自然科学基金项目(40174020)资助
摘    要:本文基于任意空间取向TI介质中坐标变换的方法,扩展研究了任意强弱、具有任意空间取向对称轴的TI介质中体波相速度和群速度的方位变化;通过模型数值计算,获得了相速度与群速度方位变化图案,并比较了二者偏差.研究发现,各向异性越强群速度与相速度的偏差越大;并且,TI对称轴的空间取向和测线方位影响速度方位变化.相对于TI对称轴,速度方位变化图案不变;但是,随着TI对称轴空间取向和测线方位的改变,其速度方位变化呈现一定的规律性.研究结果可以精确地预测任意空间取向TI介质中速度方位变化,有利于地震各向异性数据处理与解释.

关 键 词:TI介质  任意空间取向  相速度  群速度  方位变化
文章编号:1004-2903(2006)02-0524-07
收稿时间:2005-07-09
修稿时间:2005-10-08

The characteristics of velocities with azimuth variation for arbitrary spatial orientation TI media
HAO Chong-tao,YAO Chen,WANG Xun.The characteristics of velocities with azimuth variation for arbitrary spatial orientation TI media[J].Progress in Geophysics,2006,21(2):524-530.
Authors:HAO Chong-tao  YAO Chen  WANG Xun
Institution:Institute of Geology, China Seismological Bureau, Beijing 100029, China
Abstract:Based on the method of coordinates transform for arbitrary spatial orientation TI media,we expanded to study the azimuth variations of body-wave phase-velocity and group-velocity for arbitrary spatial orientation TI media with arbitrary strength of anisotropy.Using simulating calculation,we obtained the patterns of phase-velocity and group-velocity,and analyzed the deviation between group-velocity and phase-velocity.This research illustrates that the stronger is anisotropy the larger is the deviation between group-velocity and phase-velocity.The spatial orientation of TI symmetry axis and surveying line azimuth has the effect on the azimuth variation of body-wave velocities.The patterns of body-wave group-velocity and phase-velocity are fixed relative to TI symmetry axis,and exhibit certain symmetry and repetition with azimuth variation.This result can be directly predicted the azimuth variation of body-wave velocities for arbitrary spatial orientation TI media.Hence,this research benefits the data processing and interpretation of seismic anisotropy.
Keywords:TI media  arbitrary spatial orientation  phase-velocity  group-velocity  azimuth variation
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